Note: Page Numbers in Italic, E.G

Total Page:16

File Type:pdf, Size:1020Kb

Note: Page Numbers in Italic, E.G Index Note: page numbers in italic, e.g. 164, refer to figures. Page numbers in bold, e.g. 72, signify entries in tables. acritarchs, Late Cambrian age constraints on Kolguev Island 159 Bothnia, Gulf of 170 Agma 39 Botniahalvoya 208, 209 Ai Formation 19-20 Breibogen-Bockfjorden Fault 192, 208 Aldan, River 234 Brennevinst]orden 193 Aldan shield 234 Brennevinsfjorden Group 192 Amderma 2, 20 Bugrino 160 Anabar shield 234 Burzyan 30 Andr6eland 192 Burzyan Group 19-21 Andr6eland-Dicksonland Graben 192, 195-196 Buton Formation 26 Andr6eneset 208 Bystrino Group 29 Angara, River 234 Bystrynskaya Group 9-12, 12 Angara Block 234 Aral Sea 146 Caledonian Suture 59 Arkhangel'sk 2, 39, 146 Caledonides 2 palaeogeographic/palaeotectonic sketch map 49 comparison with Laurentian margin 197-200, 198 Arsha Formation 23 relationship with Timanides 201 Atomt]ella Antiform 194-195, 194, 209 western Baltoscandian basins 178, 178 Austfonna 209 type I basins 178-181,179 Avzyan Formation 22 type II basins 181 - 182 type III basins 182-183 Bad'yashorskaya Formation 148 Celsiusberget Group 193 Baikal, Lake 234 Central Timan Fault (CTF) 6, 48, 48, 60, 170 Baikalides 1,233 palaeogeographic/palaeotectonic sketch map 49 Baikibash Formation 24 Chaichiy Island 62 Bakal Formation 20-21 Chelyabinsk 2 Bakeevo Formation 23 Chelyuskin ophiolite belt 240-241 Balto-Timanian triple junction (BTTJ) 185 Chernaya, River 70 Bangenhuken Complex 194 Chernyi Kamen Formation 26 Barents Sea 2, 6, 59 Cheshskaya Bay 6, 8, 60, 70 Timanian and Caledonian trends 53-54 Chetlas Group 28 regional palaeotectonic setting in Late Permian 53 Chidvia Formation 38 Barentsian Caledonides 199 Churochnaya Formation 27 Barentsoya 208 Barmin, Cape 8, 60, 70 Damflya 193, 208 Barminskaya Group 8-9, 9 Demino Formation 26 Bashkirian Anticlinorium 19, 151,152 Dimtemyol, River 11 Lower Riphean 19- 21 Dorogor Formation 28 Middle Riphean 21-22 Dronning Louise Land 198 Upper Riphean 22-23 Duvefjorden 192, 193, 208 Lower Vendian 23 Dvina, River 2 Upper Vendian 23 Dvoretsk suite 26 stratigraphic correlation chart 21 Dzela complex 107, 121 Basinskaya Formation 151 geochemistry 112 B~tsfjord Formation 171 blueschist- and greenschist-facies rocks 113-115, 113 Belaya 20 mafic rocks 113, 113 Belaya, River 30 ultramafic rocks 112-113,113 Bellsund 192 geological setting 107-109, 108 Beloretsk 152 magmatic rocks Beloretsk Terrane 38 mafic rocks 112 Berezov 146 ultramafic rocks 109-112 Berlev~g 52 whole rock geochemical analyses 110-111 Billetjorden 192 metamorphic rocks Billel]orden Fault Zone 192, 194 amphibolite facies 112 Biri transgression 181 blueschist facies 112 Biscayerhalv6ya-Holtedahlfonna Horst 192, 196 greenschist facies 112 Bjornoya 197 petrogenesis 118-119 Bolshoy Kameshek massif 70, 71 blueschists and greenschists 119 gabbro and granite isotope dating 71-73, 72 tectonic setting 120-121 Bolshoy Rumyanichny, Cape 8, 60, 70, 71 timing 119-120 Bolvan Creek Formation 29 U-Pb dating 115-118, 115, 116, 117, 118 Bolvansky Formation 7, 8 microprobe data 114 249 Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3853989/9781862394056_backmatter.pdf by guest on 27 September 2021 250 INDEX East European Craton 19, 20 Kanin Peninsula 2, 6-8, 6, 8, 48 Precambrian geology 75-76, 76 Baltica margins 175-178, 175, 177 Riphean-Vendian tectonic and sedimentary events 31-32 compared with northern Timan and Vymskaya Ridge 12-13 lateral and vertical architecture map 31 Early Palaeozoic unconformity 145-147, 147 Vendian succession 38 Neoproterozoic high-grade metamorphism 59, 59, 67-68 East Timan Fault (ETF) 6, 48, 51, 60, 170 conditions of metamorphism 65 -67 Edge6ya 192, 208 geochronology, previous work 62-63 Ekaterinburg 2, 20, 30, 31, 146 lithologies 63 Eletskaya Facies 150, 153 metamorphism, previous work 61-62 Engane-Pe Anticline 27, 88-89, 148, 148, 149 regional geology 59-61, 60 Enganepeiskaya Group 148 sample descriptions 63 Engerdalen Basin 181 structure 63 Eolussletta Shear Zone 194 timing of metamorphism 67 Ernasalya, Cape 62 palaeogeographic/palaeotectonic sketch map 49 Eskolabreen Complex 194 thermobarometry EUROPROBE 1 analytical data and interpretation 65 biotite compositions 64 Fedotovo Formation 25 garnet compositions 64 Fl~tan-Instrumentberget Complex 194 methods 63-64 Forlandsundet 192 plagioclase compositions 65 Foynoyane 208 results 67 Franklinsundet 193 Kapitansky, Cape 8 Franldinsundet Group 193 Kapp Hansteen Group 192 Franz Josef Land 47, 59 Kara Sea 2, 47, 146, 234 Karatau Group 22-23 Garevka Formation 26 Karlin Formation 25 Glitnefonna 193 Karpinsky Peninsula 154 Gnilsk Formation 29 Katav Formation 22 Grubeinskaya Formation 149, 150 Kazan' 2 Kernos Formation 26 Hamberg Gletcher Foreland 198 Kharbei Complex 148 Hedmark 170 Khatalambinsky Suite 150 Hedmark Basin 178-181,180 Khoidyshor Formation 27 Heidal 170 Khoreyver terrane Heidal Group 181 palaeogeographic/palaeotectonic sketch map 49 Helvetesflya Formation 192 Kikvozhkaya Formation 11, 12 Hinlopenstreten 208 Kildin Island 52, 169-171, 170 Hinlopenstreten Supergroup 192, 193 Kirkenes 52 Hinlopenstretet 192, 194 Klyktan Formation 25 Hinlopenstretet Syncline 209 Kocheshor Formation 27 Homsund 192 Koiva Formation 26 Hoyvik 170 Kola Peninsula 6, 47, 170 Baltica margins 174-175 Igarka 234, 238 palaeogeographic/palaeotectonic sketch map 49 II'yavozh Formation 27 Kolguev Island 2, 48 Innvika 208 geological background 159-160, 160 Innvikhogda Syncline 209 stratigraphic levels 161 Inostrantseva Bay 141 Late Cambrian age constraints by acritarchs 159 Inta 31, 160 biostratigraphic implications 167 Inzer 30, 31 Cambrian rocks in Pechora Basin and adjacent areas 160-162 Inzer Formation 22-23 Cambrian-Ordovician successions 162-163 Is~orden 192 characterization of acritarchs 163-166, 164, 165 Ishimbai 30 previous fossil records 163 Isispynten 193, 208 study materials and methods 163 Ivdel 146 palaeogeographic/palaeotectonic sketch map 49 Izhma 31 shelly fossils 166-167, 166 Kolpakovskaya Formation 151 Jameson Land 198 Kong Karls Land 208 Kongsfjord 52 Kalak Nappe Complex 183 Kongsfjord Formation 171 Kaltasa Formation 24 Kongsfjord Turbidite System (KTS) 13, 14, 15 Kama 20 Kotlas 31 Kama, River 31 Kotlin stratohorizon 44 Kamen Rassolny Formation 26 Kozinskaya Formation 151 Kamennye Sopki massif 70 Kraemerpynten 208 Kamsk-Belsk depression 24 Krasnaya Bay 62 Kanin Kamen Ridge 6 Krasnokamsk Formation 25 Kanin Kamen Supergroup 7, 8, 15-16 Krayny Kameshek massif 70, 71 Kanin Nos Cape 6 syenite isotope dating 71-73, 72 Downloaded from http://pubs.geoscienceworld.org/books/book/chapter-pdf/3853989/9781862394056_backmatter.pdf by guest on 27 September 2021 INDEX 251 Krivaya Luka Formation 23 Makovskaya Series 141 Kronprins Christian Land 198 Malochernoretskaya Formation 8-9, 9 Kurgashlya Formation 23 Maly Kameshek massif 70 Kvaenangsfjorden 170 Man'inskaya Formation 148, 149 Kvarkush metamorphic basement 125, 132 Manitanyrdskaya Group 148, 150 ages Man'ya Formation 27 basaltic dyke 131 Marun-Keu Complex 87, 101-102 blueschist-facies metamorphism 129-131, 130 analytical procedures 90 post-Timanian processes 131 elemental chemistry 91 regional implications 131 - 132 ion microprobe zircon analyses 90-91 tectonic setting of blueschist-facies metamorphism 131 single zircon Pb evaporation 90, 91 analytical procedures 127-128 Sm-Nd and Rb-Sr analyses 91 geoloigical setting of Kvarkush Anticline 125-127, 126, 127 analytical results results 128-129, 129 comparative geochronology 99-100 sampling and sample characteristics 127 ion microprobe U-Th-Pb 92- 93 Kvarkush-Kamennogorsk Anticlinorium 25, 151 major and trace element data 95, 100 Upper Riphean 25-26 Rb-Sr whole rock data 94, 99 Lower Vendian 26 Sm-Nd data and Nd model ages 94, 98-99 Upper Vendian 26 zircon geochronology 91-97, 98, 99 Kvitoya 208 zircon images 96, 97 Kvitvola Nappe Complex 181 zircon stability in eclogite-facies metamorphism 97 Kyiv 38 geological setting 87-90, 88, 89 Kykva Formation 25 lithologies and sampling 90 Kykvozh Formation 29 regional correlations and geodynamic interpretation 100 Kyrmin Formation 25 Baltica passive margin rifting 101 Kyrpin Group 24 Early Timanian evolution 100 Kyzgey Formation 27 Uralian convergence and arc-continent collision 101 sample characterization 102 Lady Franklinfjorden 193 Mashak Formation 21 - 22 L~g6ya 193 Matochkin Strait 154 Laksefjord Nappe Complex 182 Matusalya, Cape 62 Lakset~orden 170 Mezen 31 Lambert Land 198 Mezen Basin 37, 38, 43, 44, 47 Lamtsa 39 Mezen Formation 28 Lamtsa-Verkovka depositional sequence 41-43 Mikulkin Antiform 61, 62 Laponiahalvrya 193, 208, 209 thermobarometry 66 Laptev Sea 59, 234 Mikulkin, Cape 6, 62 Laptopay Formation 27 Mikulkino Group 29 Las'va Group 25 Mikulkinskaya Group 6, 7, 61, 66 Laurentian margin 191,203 Minsk 38 comparison with East Greenland Caledonides 197-200, 198 Minyar Formation 23 comparison with North Greenland fold belt and Pearya 199, Mitushikha Bay 140 200-201,202 Mityushev Kamen' Massif 153 Svalbard 191 Moelv Tillite 180-181 assembly of terranes 201 Mongol-Okhotsk belt 234 Bjomoya 197 Morozovskaya Formation 153 eastern terranes 191-195 Moscow 38 interrelationships between the terranes 197 Moscow Basin 38, 43-44, 44 northern terranes 195-196 Motalat]ellet 192 relationship between Caledonides and Timanides 201 Murchisont]orden Supergroup 192, 193 southwestern terranes 196-197 Murmansk 2, 52, 146 Leaonidovo Formation 24 Lemvinskaya Facies 150 Nadezhdino Formation 24 Lena, River 234 Nafta Formation 28 Lom0orden Fault 192, 194 Nar'yan-Mar 2, 31 Lomfjorden Supergroup 192 Nenoxa Formation 38 Lomonosov
Recommended publications
  • Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) Professional Paper
    Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) Professional Paper Chapter A of The 2008 Circum-Arctic Resource Appraisal Professional Paper 1824 U.S. Department of the Interior U.S. Geological Survey Cover. View to the east of the Lisburne well during active drilling in July 1979, Ivotuk Hills, northern Alaska. U.S. Geological Survey photo by Thomas Moore. Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) Professional Paper By Donald L. Gautier and Thomas E. Moore Chapter A of The 2008 Circum-Arctic Resource Appraisal Edited by T.E. Moore and D.L. Gautier Professional Paper 1824 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey William H. Werkheiser, Acting Director U.S. Geological Survey, Reston, Virginia: 2017 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Gautier, D.L., and Moore, T.E., 2017, Introduction to the 2008 Circum-Arctic Resource Appraisal (CARA) professional paper, chap.
    [Show full text]
  • Ediacaran) of Earth – Nature’S Experiments
    The Early Animals (Ediacaran) of Earth – Nature’s Experiments Donald Baumgartner Medical Entomologist, Biologist, and Fossil Enthusiast Presentation before Chicago Rocks and Mineral Society May 10, 2014 Illinois Famous for Pennsylvanian Fossils 3 In the Beginning: The Big Bang . Earth formed 4.6 billion years ago Fossil Record Order 95% of higher taxa: Random plant divisions domains & kingdoms Cambrian Atdabanian Fauna Vendian Tommotian Fauna Ediacaran Fauna protists Proterozoic algae McConnell (Baptist)College Pre C - Fossil Order Archaean bacteria Source: Truett Kurt Wise The First Cells . 3.8 billion years ago, oxygen levels in atmosphere and seas were low • Early prokaryotic cells probably were anaerobic • Stromatolites . Divergence separated bacteria from ancestors of archaeans and eukaryotes Stromatolites Dominated the Earth Stromatolites of cyanobacteria ruled the Earth from 3.8 b.y. to 600 m. [2.5 b.y.]. Believed that Earth glaciations are correlated with great demise of stromatolites world-wide. 8 The Oxygen Atmosphere . Cyanobacteria evolved an oxygen-releasing, noncyclic pathway of photosynthesis • Changed Earth’s atmosphere . Increased oxygen favored aerobic respiration Early Multi-Cellular Life Was Born Eosphaera & Kakabekia at 2 b.y in Canada Gunflint Chert 11 Earliest Multi-Cellular Metazoan Life (1) Alga Eukaryote Grypania of MI at 1.85 b.y. MI fossil outcrop 12 Earliest Multi-Cellular Metazoan Life (2) Beads Horodyskia of MT and Aust. at 1.5 b.y. thought to be algae 13 Source: Fedonkin et al. 2007 Rise of Animals Tappania Fungus at 1.5 b.y Described now from China, Russia, Canada, India, & Australia 14 Earliest Multi-Cellular Metazoan Animals (3) Worm-like Parmia of N.E.
    [Show full text]
  • Contributions to the Neoproterozoic Geobiology
    Contributions to the Neoproterozoic Geobiology Bing Shen Dissertation submitted to the faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy In Department of Geosciences Shuhai Xiao (Chair) Robert Bodnar Michal Kowalewski J. Fred Read November 29, 2007 Blacksburg, Virginia Key words: Neoproterozoic, Ediacaran, Ediacara fossils, China, Disparity, Sulfur isotope, Carbon isotope Copyright 2007, Bing Shen Contributions to the Neoproterozoic Geobiology Bing Shen Abstract This thesis makes several contributions to improve our understanding of the Neoproterozoic Paleobiology. In chapter 1, a comprehensive quantitative analysis of the Ediacara fossils indicates that the oldest Ediacara assemblage—the Avalon assemblage— already encompassed the full range of Ediacara morphospace. A comparable morphospace range was occupied by the subsequent White Sea and Nama assemblages, although it was populated differently. In contrast, taxonomic richness increased in the White Sea assemblage and declined in the Nama assemblage. The Avalon morphospace expansion mirrors the Cambrian explosion, and both may reflect similar underlying mechanisms. Chapter 2 describes problematic macrofossils collected from the Neoproterozoic slate of the upper Zhengmuguan Formation in North China and sandstone of the Zhoujieshan Formation in Chaidam. Some of these fossils were previously interpreted as animal traces. Our study of these fossils recognizes four genera and five species. None of these taxa can be interpreted as animal traces. Instead, they are problematic body fossils of unresolved phylogenetic affinities. Chapter 3 reports stable isotopes of the Zhamoketi cap dolostone atop the Tereeken diamictite in the Quruqtagh area, eastern Chinese Tianshan. Our new data indicate that carbonate associated sulfate (CAS) abundance decreases rapidly in the basal 34 cap dolostone and δ SCAS composition varies between +9‰ and +15‰ in the lower 2.5 34 m.
    [Show full text]
  • Systemic Criteria for the Evaluation of the Role of Monofunctional Towns in the Formation of Local Urban Agglomerations
    ISSN 2007-9737 Systemic Criteria for the Evaluation of the Role of Monofunctional Towns in the Formation of Local Urban Agglomerations Pavel P. Makagonov1, Lyudmila V. Tokun2, Liliana Chanona Hernández3, Edith Adriana Jiménez Contreras4 1 Russian Presidential Academy of National Economy and Public Administration, Russia 2 State University of Management, Finance and Credit Department, Russia 3 Instituto Politécnico Nacional, Escuela Superior de Ingeniería Mecánica y Eléctrica, Mexico 4 Instituto Politécnico Nacional, Escuela Superior de Cómputo, Mexico [email protected], [email protected], [email protected] Abstract. There exist various federal and regional monotowns do not possess any distinguishing self- programs aimed at solving the problem of organization peculiarities in comparison to other monofunctional towns in the periods of economic small towns. stagnation and structural unemployment occurrence. Nevertheless, people living in such towns can find Keywords. Systemic analysis, labor migration, labor solutions to the existing problems with the help of self- market, agglomeration process criterion, self- organization including diurnal labor commuting migration organization of monotown population. to the nearest towns with a more stable economic situation. This accounts for the initial reason for agglomeration processes in regions with a large number 1 Introduction of monotowns. Experimental models of the rank distribution of towns in a system (region) and evolution In this paper, we discuss the problems of criteria of such systems from basic ones to agglomerations are explored in order to assess the monotown population using as an example several intensity of agglomeration processes in the systems of monotowns located in Siberia (Russia). In 2014 the towns in the Middle and Southern Urals (the Sverdlovsk Government of the Russian Federation issued two and Chelyabinsk regions of Russia).
    [Show full text]
  • The Mineral Indutry of Russia in 1998
    THE MINERAL INDUSTRY OF RUSSIA By Richard M. Levine Russia extends over more than 75% of the territory of the According to the Minister of Natural Resources, Russia will former Soviet Union (FSU) and accordingly possesses a large not begin to replenish diminishing reserves until the period from percentage of the FSU’s mineral resources. Russia was a major 2003 to 2005, at the earliest. Although some positive trends mineral producer, accounting for a large percentage of the were appearing during the 1996-97 period, the financial crisis in FSU’s production of a range of mineral products, including 1998 set the geological sector back several years as the minimal aluminum, bauxite, cobalt, coal, diamonds, mica, natural gas, funding that had been available for exploration decreased nickel, oil, platinum-group metals, tin, and a host of other further. In 1998, 74% of all geologic prospecting was for oil metals, industrial minerals, and mineral fuels. Still, Russia was and gas (Interfax Mining and Metals Report, 1999n; Novikov significantly import-dependent on a number of mineral products, and Yastrzhembskiy, 1999). including alumina, bauxite, chromite, manganese, and titanium Lack of funding caused a deterioration of capital stock at and zirconium ores. The most significant regions of the country mining enterprises. At the majority of mining enterprises, there for metal mining were East Siberia (cobalt, copper, lead, nickel, was a sharp decrease in production indicators. As a result, in the columbium, platinum-group metals, tungsten, and zinc), the last 7 years more than 20 million metric tons (Mt) of capacity Kola Peninsula (cobalt, copper, nickel, columbium, rare-earth has been decommissioned at iron ore mining enterprises.
    [Show full text]
  • Great Siberian Highway and Process Urbanization on Southern Ural (1891-1914 Years)
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Siberian Federal University Digital Repository Journal of Siberian Federal University. Humanities & Social Sciences 2 (2009 2) 176-183 ~ ~ ~ УДК 908 Great Siberian Highway and Process Urbanization on Southern Ural (1891-1914 Years) Aleksandr A. Timofeev* South-Ural state university, 76 Lenin av., Chelyabinsk, 454080 Russia 1 Received 23.03.2009, received in revised form 30.03.2009, accepted 6.04.2009 There are considered urban population’s processes occurring on Southern Ural after construction of the Transsiberian railway (Transsib) at the end of XIX – the beginning of XX centuries in clause. The reasons of strengthening of the urbanization process , the increase of the urban population’s share on Southern Ural were growth of industry and trade, requirement for a cheap labour. Ufa, Zlatoust, Chelyabinsk cities, located along the Transsiberian railway, become the large railway stations. Keywords: Transsiberian railway, Southern Ural, urbanization, modernization. The considered period of 1891-1914 it is communication networks in the urbanized possible to characterize as an initial stage the territories. Modernization, «industrialization, urbanization’s transition of the Southern-Ural urbanization frequently proceed in interrelation». region. The essence of a urbanization consists In conditions of modernization of the end XIX – in territorial concentration of the human the beginnings XX centuries cities concentrated activity, conducting to the intensification and in themselves economic, administrative, differentiations down to allocation of new scientific, spiritual potential of all society. The city forms and spatial structures of population economic maintenance of modernization consists moving. Urban transition is qualitatively in development industrial, transport, trading, allocated, supreme stage of the urbanization’s financial-bank systems and other kinds of not process, which conducts to radical transformation agricultural branches.
    [Show full text]
  • Traces of Locomotion of Ediacaran Macroorganisms
    geosciences Article Traces of Locomotion of Ediacaran Macroorganisms Andrey Ivantsov 1,* , Aleksey Nagovitsyn 2 and Maria Zakrevskaya 1 1 Laboratory of the Precambrian Organisms, Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow 117997, Russia; [email protected] 2 Arkhangelsk Regional Lore Museum, Arkhangelsk 163000, Russia; [email protected] * Correspondence: [email protected] Received: 21 August 2019; Accepted: 4 September 2019; Published: 11 September 2019 Abstract: We describe traces of macroorganisms in association with the body imprints of trace-producers from Ediacaran (Vendian) deposits of the southeastern White Sea region. They are interpreted as traces of locomotion and are not directly related to a food gathering. The complex remains belong to three species: Kimberella quadrata, Dickinsonia cf. menneri, and Tribrachidium heraldicum. They were found in three different burials. The traces have the form of narrow ridges or wide bands (grooves and linear depressions on natural imprints). In elongated Kimberella and Dickinsonia, the traces are stretched parallel to the longitudinal axis of the body and extend from its posterior end. In the case of the isometric Tribrachidium, the trace is directed away from the margin of the shield. A short length of the traces indicates that they were left by the organisms that were covered with the sediment just before their death. The traces overlaid the microbial mat with no clear signs of deformation under or around the traces. A trace substance, apparently, differed from the material of the bearing layers (i.e., a fine-grained sandstone or siltstone) and was not preserved on the imprints. This suggests that the traces were made with organic material, probably mucus, which was secreted by animals in a stressful situation.
    [Show full text]
  • Cephalonega, a New Generic Name, and the System of Vendian Proarticulata A
    ISSN 0031-0301, Paleontological Journal, 2019, Vol. 53, No. 5, pp. 447–454. © Pleiades Publishing, Ltd., 2019. Russian Text © The Author(s), 2019, published in Paleontologicheskii Zhurnal, 2019, No. 5, pp. 14–21. Cephalonega, A New Generic Name, and the System of Vendian Proarticulata A. Yu. Ivantsova, *, M. A. Fedonkina, A. L. Nagovitsynb, and M. A. Zakrevskayaa aBorissiak Paleontological Institute, Russian Academy of Sciences, Moscow, 117647 Russia bArkhangelsk Office, Russian Geographical Society, Russian Academy of Sciences, Arkhangelsk, 163001 Russia *e-mail:[email protected] Received December 29, 2017; revised November 9, 2018; accepted February 14, 2019 Abstract—Due to homonymy, a new name Cephalonega Fedonkin, nom. nov. was proposed for the genus of Vendian macroorganisms, Onega Fedonkin. The improved diagnosis of this genus and evidence that this genus belongs to Proarticulata, an extinct phylum of Metazoa, are given. A detailed characterization of the phylum and all Proarticulata classes is given for the first time. Keywords: Late Vendian, Ediacaran, Proarticulata, Vendiamorpha, Dipleurozoa, Cephalozoa, Onega, Ceph- alonega DOI: 10.1134/S0031030119050046 INTRODUCTION the genus and the description of the species were mod- In 1972 the first large locality of Ediacaran-type ified. In order to substantiate the systematical position fossils in the Upper Vendian natural outcrops in the of the taxon the refined characteristics of Proarticulata north-west of the East European Platform was discov- and subordinated high-rank taxa were formulated. ered on the Onega Peninsula along the banks of the Syuzma River (Keller et al., 1974). At the early stages DISCUSSION of studying the Syuzma locality, several impressions of a small organism were found and this organism was The phylum Proarticulata was distinguished in the described as the monotypical genus Onega Fedonkin, composition of the Vendian fauna on the basis of 1976 (Keller and Fedonkin, 1976).
    [Show full text]
  • Turkic Toponyms of Eurasia BUDAG BUDAGOV
    BUDAG BUDAGOV Turkic Toponyms of Eurasia BUDAG BUDAGOV Turkic Toponyms of Eurasia © “Elm” Publishing House, 1997 Sponsored by VELIYEV RUSTAM SALEH oglu T ranslated by ZAHID MAHAMMAD oglu AHMADOV Edited by FARHAD MAHAMMAD oglu MUSTAFAYEV Budagov B.A. Turkic Toponyms of Eurasia. - Baku “Elm”, 1997, -1 7 4 p. ISBN 5-8066-0757-7 The geographical toponyms preserved in the immense territories of Turkic nations are considered in this work. The author speaks about the parallels, twins of Azerbaijani toponyms distributed in Uzbekistan, Kazakhstan, Turkmenistan, Altay, the Ural, Western Si­ beria, Armenia, Iran, Turkey, the Crimea, Chinese Turkistan, etc. Be­ sides, the geographical names concerned to other Turkic language nations are elucidated in this book. 4602000000-533 В ------------------------- 655(07)-97 © “Elm” Publishing House, 1997 A NOTED SCIENTIST Budag Abdulali oglu Budagov was bom in 1928 at the village o f Chobankere, Zangibasar district (now Masis), Armenia. He graduated from the Yerevan Pedagogical School in 1947, the Azerbaijan State Pedagogical Institute (Baku) in 1951. In 1955 he was awarded his candidate and in 1967 doctor’s degree. In 1976 he was elected the corresponding-member and in 1989 full-member o f the Azerbaijan Academy o f Sciences. Budag Abdulali oglu is the author o f more than 500 scientific articles and 30 books. Researches on a number o f problems o f the geographical science such as geomorphology, toponymies, history o f geography, school geography, conservation o f nature, ecology have been carried out by academician B.A.Budagov. He makes a valuable contribution for popularization o f science.
    [Show full text]
  • BR IFIC N° 2611 Index/Indice
    BR IFIC N° 2611 Index/Indice International Frequency Information Circular (Terrestrial Services) ITU - Radiocommunication Bureau Circular Internacional de Información sobre Frecuencias (Servicios Terrenales) UIT - Oficina de Radiocomunicaciones Circulaire Internationale d'Information sur les Fréquences (Services de Terre) UIT - Bureau des Radiocommunications Part 1 / Partie 1 / Parte 1 Date/Fecha 22.01.2008 Description of Columns Description des colonnes Descripción de columnas No. Sequential number Numéro séquenciel Número sequencial BR Id. BR identification number Numéro d'identification du BR Número de identificación de la BR Adm Notifying Administration Administration notificatrice Administración notificante 1A [MHz] Assigned frequency [MHz] Fréquence assignée [MHz] Frecuencia asignada [MHz] Name of the location of Nom de l'emplacement de Nombre del emplazamiento de 4A/5A transmitting / receiving station la station d'émission / réception estación transmisora / receptora 4B/5B Geographical area Zone géographique Zona geográfica 4C/5C Geographical coordinates Coordonnées géographiques Coordenadas geográficas 6A Class of station Classe de station Clase de estación Purpose of the notification: Objet de la notification: Propósito de la notificación: Intent ADD-addition MOD-modify ADD-ajouter MOD-modifier ADD-añadir MOD-modificar SUP-suppress W/D-withdraw SUP-supprimer W/D-retirer SUP-suprimir W/D-retirar No. BR Id Adm 1A [MHz] 4A/5A 4B/5B 4C/5C 6A Part Intent 1 107125602 BLR 405.6125 BESHENKOVICHI BLR 29E28'13'' 55N02'57'' FB 1 ADD 2 107125603
    [Show full text]
  • Eunaseis: a Seismic Model for Moho and Crustal Structure in Europe, Greenland, and the North Atlantic Region
    EUNAseis a seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region Artemieva, Irina; Thybo, Hans Published in: Tectonophysics DOI: 10.1016/j.tecto.2013.08.004 Publication date: 2013 Document version Publisher's PDF, also known as Version of record Citation for published version (APA): Artemieva, I., & Thybo, H. (2013). EUNAseis: a seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region. Tectonophysics, 609, 97-153. https://doi.org/10.1016/j.tecto.2013.08.004 Download date: 04. Oct. 2021 Tectonophysics 609 (2013) 97–153 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Review Article EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region☆ Irina M. Artemieva ⁎, Hans Thybo IGN, University of Copenhagen, Denmark article info abstract Article history: We present a new digital crustal model for Moho depth and crustal structure in Europe, Greenland, Iceland, Received 27 November 2012 Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W–62E, 30N–84N). Our compilation is based Received in revised form 18 July 2013 on digitization of original seismic profiles and Receiver Functions from ca. 650 publications which provides a Accepted 4 August 2013 dense regional data coverage. Exclusion of non-seismic data allows application of the database to potential Available online 15 August 2013 field modeling. EUNAseis model includes Vp velocity and thickness of five crustal layers, including the sedimen- tary cover, and Pn velocity. For each parameter we discuss uncertainties associated with theoretical limitations, Keywords: Moho regional data quality, and interpolation.
    [Show full text]
  • SUPERSONIC ENERGY Business Report
    2009 INTERREGIONAL DISTRIBUTIVE G RID C OMPANY IDG C OF URALS SUPERSONIC ENERGY business report Back to Contents >> Key financial indicators1 2009 2009 20082 (US$, thous.) (RUR, thous.) (RUR, thous.) Revenues, including 1 299 894.1 41 297 636 35 964 707 transmission revenues 1 259 086.4 40 001 176 34 437 161 connection revenues 30 657.4 973 985 895 581 Expenses 1 152 773.4 36 623 611 33 947 171 Operating profit 147 120.7 4 674 025 2 017 536 Operating margin, % 11.3% 11.3% 5.6% EBITDA3 131 941.8 4 191 790 3 576 138 EBITDA margin, % 10.2% 10.2% 9.9% Pre-tax income 43 845.5 1 392 972 1 288 425 Net profit 33 152.9 1 053 267 862 085 Net margin, % 2.6% 2.6% 2.4% Earnings per share US$ 0.0003 RUR 0.01 RUR 0.02 Short-term loans and borrowings 0 0 1 200 000 Long-term loans and borrowings 175 749.5 5 583 562 5 161 534 bonds 51.6 1 638 1 000 000 Debt/ Equity, % 20% 20% 23% Equity/ Assets, % 66% 66% 66% Energy sales 2009 2008 Change, % Energy supply, mln kW/h 75 795.9 86 365.8 - 12.24 Productive supply, mln kW/h 69 339.2 79 902 - 13.22 1 Key financial indicators of the Company are represented on the basis of 2008-2009 Operating figures 2009 audited financial statements under Russian Accounting Aerial lines (in chains), km 122 054 Standards (RAS). 2009 indica- tors were shown in US dollars Aerial lines (in lines), km 113 210 just for information (average rate as of 2009 is 1US$= RUR Cable lines, km 4 691 31.77).
    [Show full text]